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Assessing the Style of Advance and Retreat of the Des Moines Lobe Using Lidar Topographic Data Sarah Elizabeth Day Iowa State University

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Assessing the Style of Advance and Retreat of the Des Moines Lobe Using Lidar Topographic Data Sarah Elizabeth Day Iowa State University Iowa State University Capstones, Theses and Graduate Theses and Dissertations Dissertations 2014 Assessing the style of advance and retreat of the Des Moines Lobe using LiDAR topographic data Sarah Elizabeth Day Iowa State University Follow this and additional works at: https://lib.dr.iastate.edu/etd Part of the Geology Commons, and the Geomorphology Commons Recommended Citation Day, Sarah Elizabeth, "Assessing the style of advance and retreat of the Des Moines Lobe using LiDAR topographic data" (2014). Graduate Theses and Dissertations. 13653. https://lib.dr.iastate.edu/etd/13653 This Thesis is brought to you for free and open access by the Iowa State University Capstones, Theses and Dissertations at Iowa State University Digital Repository. It has been accepted for inclusion in Graduate Theses and Dissertations by an authorized administrator of Iowa State University Digital Repository. For more information, please contact [email protected]. Assessing the style of advance and retreat of the Des Moines Lobe using LiDAR topographic data by Sarah Elizabeth Day A thesis submitted to the graduate faculty in partial fulfillment of the requirements for the degree of MASTER OF SCIENCE Major: Geology Program of Study Committee: Neal R. Iverson, Major Professor Chris Harding William W. Simpkins Iowa State University Ames, Iowa 2014 Copyright © Sarah Elizabeth Day, 2014. All rights reserved ii TABLE OF CONTENTS Page ACKNOWLEDGEMENTS ...................................................................................... iii ABSTRACT .............................................................................................................. iv CHAPTER 1 INTRODUCTION .......................................................................... 1 A. The Des Moines Lobe ................................................................................... 1 B. Motivation and hypothesis ............................................................................ 15 C. Objectives ...................................................................................................... 16 CHAPTER 2 METHODS ..................................................................................... 18 A. Introduction ................................................................................................... 18 B. LiDAR ........................................................................................................ 19 C. Mapping methodology .................................................................................. 20 D. Testing retreat hypothesis .............................................................................. 29 CHAPTER 3 RESULTS ....................................................................................... 32 A. Mapping ....................................................................................................... 32 B. Relationship of minor moraines to end moraines .......................................... 42 CHAPTER 4 DISCUSSION ................................................................................ 58 A. Evidence of stagnation .................................................................................. 58 B. Significance of minor moraine orientations ................................................ 62 C. Lack of flow-parallel features ....................................................................... 64 D. Modern analog ............................................................................................... 67 CHAPTER 5 CONCLUSIONS ............................................................................ 70 REFERENCES .......................................................................................................... 72 iii ACKNOWLEDGEMENTS I would like to thank some of the people who helped me with this research and guided me through the writing process. First, I’d like to thank my advisor, Neal Iverson, for his guidance and patience throughout the entire research process. His insight and attention to detail have helped me make this thesis something I can be proud of. Furthermore, given the additional responsibilities he took on as department chair, the amount of time he spent helping me with research and writing is astounding. Next, I’d like to thank Lucas Zoet, Neal’s post-doc, who helped me appreciate the power of computer coding. He helped me process much of my data, and without his vast knowledge of different programing platforms, this research would not have been completed. In addition, I would also like to thank a few other people who have helped me throughout this process. I’d like to thank the second and third members of my Program of Study committee, Chris Harding and Bill Simpkins, for their time and effort in perfecting this project. I would like to thank DeAnn Frisk, the department administrative specialist, for her patience, knowledge, and support. I would also like to thank the rest of the Iowa State geology department for making my time as a graduate student successful and enjoyable. Finally, I’d like to thank my friends and family for supporting me even when I was frustrated. Without their love and support through the entire process I would not have been able to finish this journey as a graduate student. iv ABSTRACT Successive advances of the late-Wisconsinan Des Moines Lobe to form three major end moraines in Iowa—sequentially the Bemis, Altamont, and Algona moraines—are thought to be the result of the lobe surging out of balance with a warming climate. Various styles of hummocky topography, collectively sometimes called stagnation moraine, are interpreted to be the result of widespread stagnation and down-wasting of ice following surges. Alternatively, end moraines could be recessional—a result of incremental back-wasting of the glacier margin and unrelated to surging. To study the retreat style of the Des Moines Lobe, high resolution LiDAR data were used to re-evaluate the subtle landscape of the lobe’s footprint in Iowa. Results indicate that ~90% of the lobe’s area, excluding major Holocene stream drainages, consists of stagnation features. Some landforms are more prevalent than mapped previously, including eskers and features interpreted to be subdued ice-walled lake plains. Importantly, subglacially formed minor moraines (a.k.a. washboard moraines), which resulted from sediment filling of transverse crevasses, cover ~60% of the lobe’s area with stagnation landforms. Also, ~25 previously unmapped end moraine ridges have been identified. Transverse crevasse-fill ridges in the forefields of modern glaciers form due to longitudinal ice extension associated with surging and are not found in the forefields of non-surge-type glaciers, so minor moraines are good evidence of Des Moines Lobe surges. Most end moraines have minor moraine sets associated with them, consistent v with a surge-like advances, and many areas have multiple sets of minor moraines indicating a surge history more complicated than one advance for each of the three major end moraines. Therefore, asserting stagnation and down-wasting after three surge-like advances provides an incomplete characterization of the Des Moines Lobe’s advance and retreat. The surge-type Bering Glacier in Alaska is a good but imperfect modern analog for the lobe. 1 CHAPTER 1: INTRODUCTION A. The Des Moines Lobe The Des Moines Lobe, the largest of the lobes along the southern margin of the Laurentide Ice Sheet (Fig. 1.1) during the last glacial maximum, advanced south into a relatively warm, boreal climate (Clark, 1994; Hooyer & Iverson, 2002; Mickelson & Colgan, 2003). At its maximum extent at approximately 13,800 14C yr BP, the lobe covered more than 100,000 km2 in southern Minnesota and north-central Iowa and extended 600 km beyond the main body of the Laurentide Ice Sheet (Mathews, 1974; Clayton & Moran, 1982; Patterson, 1997; Hooyer & Iverson, 2002). The lobe had retreated from Iowa by 11,700 14C yr BP (Clayton & Moran, 1982). a b Figure 1.1: a. Maximum extents of the Laurentide Ice Sheet and Cordilleran Ice Sheets during the late Wisconsinan and during earlier Quaternary glaciations (Illinois State Geological Survey, 2008). b. Extent of the southern Laurentide Ice Sheet lobes in the western Midwest ~13,800 radiocarbon years ago (Hooyer & Iverson, 2002). A detailed chronology of the Des Moines Lobe in Iowa is well established by radiocarbon dates from trees overridden by the glacier and buried in till (Kemmis et al. 1981; Clayton & Moran, 1982). The Bemis (13,800 14C yr BP), Altamont (13,500 14C yr 2 BP), and Algona (12,300 14C yr BP) end moraines (Fig. 1.2) mark three major advances of the lobe (Ruhe, 1969; Kemmis et al., 1981). These moraines are broad, 1-10 km wide, swaths of hummocky topography characterized by linked-depressions, kames, ice- walled lake plains, and elongate flow parallel ridges (Kemmis, 1991). Figure 1.2: Iowa footprint of the Des Moines Lobe. The three major end moraines are the Bemis, Altamont, and Algona, delimited by areas of hummocky topography. The moraine complex includes areas where the moraines merge laterally. Paleoglaciology Reconstructions of the Des Moines Lobe using modern moraine elevations and minor moraines to indicate flow direction indicate the lobe’s probable geometry at its maximum extent (Clark, 1992; Iverson and Hooyer, 2002). The lobe was unusually thin 3 and gently sloping. Clark (1992) calculated its thickness to be only 300 m, 275 km up- glacier from the terminus, a factor of ~10 thinner than the margin of the Greenland Ice Sheet. Hooyer and Iverson
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